Iceland is primarily located on the Mid-Atlantic Ridge, which is a divergent boundary where the North American and Eurasian tectonic plates are moving apart. This geological setting allows for volcanic activity and the formation of new crust. Additionally, Iceland sits above a hotspot, which contributes to its high levels of volcanic activity and geothermal energy. Therefore, Iceland is both a divergent boundary and a hotspot.
rezy
Vesuvius is associated with a convergent boundary between the African Plate and the Eurasian Plate.
Iceland, (The mid-atlantic Ridge)
Mount Katmai is located on a convergent plate boundary.
A hot spot is not associated with a plate boundary.
Krakatoa is located at a convergent boundary, where the Indo-Australian Plate is being subducted beneath the Eurasian Plate. This subduction zone can lead to intense volcanic activity due to the melting and rising of magma from the subducted plate.
It is not on a plate boundary. Therefore it may be on hotspot.
Costa Rica is a convergent plate boundary, specifically a subduction zone where the Cocos Plate is being subducted beneath the Caribbean Plate. This geologic process is responsible for the country's high levels of seismic and volcanic activity.
The Ol Doinyo Lengai volcano is located in Tanzania near the East African Rift, which is a divergent boundary where tectonic plates are moving away from each other. This rift is part of the larger East African Rift System, where new crust is being formed as the African Plate splits into the Nubian Plate and the Somali Plate.
hot spot
Mount St Helens is on a convergent plate boundary.
Yes, Iceland was formed from the interaction of the North American and Eurasian tectonic plates. The divergent boundary between these two plates causes volcanic activity that has led to the formation of Iceland.